CLONING AND SEQUENCING OF THE GENE ENCODING GLUTAMINE SYNTHETASE-I FROM THE ARCHAEUM PYROCOCCUS-WOESEI - ANOMALOUS PHYLOGENIES INFERRED FROM ANALYSIS OF ARCHAEAL AND BACTERIAL GLUTAMINE SYNTHETASE-I SEQUENCES
O. Tiboni et al., CLONING AND SEQUENCING OF THE GENE ENCODING GLUTAMINE SYNTHETASE-I FROM THE ARCHAEUM PYROCOCCUS-WOESEI - ANOMALOUS PHYLOGENIES INFERRED FROM ANALYSIS OF ARCHAEAL AND BACTERIAL GLUTAMINE SYNTHETASE-I SEQUENCES, Journal of bacteriology, 175(10), 1993, pp. 2961-2969
The gene glnA encoding glutamine synthetase I (GSI) from the archaeum
Pyrococcus woesei was cloned and sequenced with the Sulfolobus solfata
ricus glnA gene as the probe. An operon reading frame of 448 amino aci
ds was identified within a DNA segment of 1,528 bp. The encoded protei
n was 49% identical with the GSI of Methanococcus voltae and exhibited
conserved regions characteristic of the GSI family. The P. woesei GSI
was aligned with available homologs from other archaea (S. solfataric
us, M. voltae) and with representative sequences from cyanobacteria, p
roteobacteria, and gram-positive bacteria. Phylogenetic trees were con
structed from both the amino acid and the nucleotide sequence alignmen
ts. In accordance with the sequence similarities, archaeal and bacteri
al sequences did not segregate on a phylogeny. On the basis of sequenc
e signatures, the GSI trees could be subdivided into two ensembles. On
e encompassed the GSI of cyanobacteria and proteobacteria, but also th
at of the high-G+C gram-positive bacterium Streptomyces coelicolor (al
l of which are regulated by the reversible adenylylation of the enzyme
subunits); the other embraced the GSI of the three archaea as well as
that of the low-G+C gram-positive bacteria (Clostridium acetobutilycu
m, Bacillus subtilis) and Thermotoga maritima (none of which are regul
ated by subunit adenylylation). The GSIs of the Thermotoga and the Bac
illus-Clostridium lineages shared a direct common ancestor with that o
f P. woesei and the methanogens and were unrelated to their homologs f
rom cyanobacteria, proteobacteria, and S. coelicolor. The possibility
is presented that the GSI gene arose among the archaea and was then la
terally transferred from some early methanogen to a Thermotoga-like or
ganism. However, the relationship of the cyanobacterial-proteobacteria
l GSIs to the Thermotoga GSI and the GSI of low-G+C gram-positive bact
eria remains unexplained.